A detailed analysis of the rapid changes in ice-core parameters during the last ice age

Results from deep Greenland ice cores show rapid changes in several parameters in the deepest part. The most probable explanation for these variations is a fast-changing climate during part of the last glaciation. The question arises, however, of whether the observed changes in the ice cores could a...

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Published in:Annals of Glaciology
Main Authors: Staffelbach, T., Stauffer, B., Oeschger, H.
Format: Conference Object
Language:English
Published: International Glaciological Society 1988
Subjects:
Online Access:https://boris.unibe.ch/158762/1/a-detailed-analysis-of-the-rapid-changes-in-ice-core-parameters-during-the-last-ice-age.pdf
https://boris.unibe.ch/158762/
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spelling ftunivbern:oai:boris.unibe.ch:158762 2023-08-20T03:59:48+02:00 A detailed analysis of the rapid changes in ice-core parameters during the last ice age Staffelbach, T. Stauffer, B. Oeschger, H. 1988 application/pdf https://boris.unibe.ch/158762/1/a-detailed-analysis-of-the-rapid-changes-in-ice-core-parameters-during-the-last-ice-age.pdf https://boris.unibe.ch/158762/ eng eng International Glaciological Society https://boris.unibe.ch/158762/ info:eu-repo/semantics/restrictedAccess Staffelbach, T.; Stauffer, B.; Oeschger, H. (1988). A detailed analysis of the rapid changes in ice-core parameters during the last ice age. Annals of glaciology, 10, pp. 167-170. International Glaciological Society 10.3189/S0260305500004377 <http://dx.doi.org/10.3189/S0260305500004377> 530 Physics info:eu-repo/semantics/conferenceObject info:eu-repo/semantics/publishedVersion PeerReviewed 1988 ftunivbern https://doi.org/10.3189/S0260305500004377 2023-07-31T22:08:19Z Results from deep Greenland ice cores show rapid changes in several parameters in the deepest part. The most probable explanation for these variations is a fast-changing climate during part of the last glaciation. The question arises, however, of whether the observed changes in the ice cores could also be due to, or at least be influenced by, discontinuities in the stratigraphy. We present new CO2 and δ18O data from the Camp Century and Dye 3 deep ice cores. The data show rapid changes in CO2 and δ18O in both cores. One transition which was investigated in detail seems to be more rapid in the ice core from Dye 3 than in the Camp Century core. The broadening of a sharp δ18O transition due to molecular diffusion is discussed. Since this broadening is larger than the observed width of the transition, we discuss the possibility of a mechanism that can produce stratigraphic disturbances on a small scale. This mechanism is based on a calculation of the compression of horizontal layers which have equal density but different viscosities. Conference Object Annals of Glaciology Dye 3 Dye-3 Greenland Greenland ice cores ice core BORIS (Bern Open Repository and Information System, University of Bern) Greenland Annals of Glaciology 10 167 170
institution Open Polar
collection BORIS (Bern Open Repository and Information System, University of Bern)
op_collection_id ftunivbern
language English
topic 530 Physics
spellingShingle 530 Physics
Staffelbach, T.
Stauffer, B.
Oeschger, H.
A detailed analysis of the rapid changes in ice-core parameters during the last ice age
topic_facet 530 Physics
description Results from deep Greenland ice cores show rapid changes in several parameters in the deepest part. The most probable explanation for these variations is a fast-changing climate during part of the last glaciation. The question arises, however, of whether the observed changes in the ice cores could also be due to, or at least be influenced by, discontinuities in the stratigraphy. We present new CO2 and δ18O data from the Camp Century and Dye 3 deep ice cores. The data show rapid changes in CO2 and δ18O in both cores. One transition which was investigated in detail seems to be more rapid in the ice core from Dye 3 than in the Camp Century core. The broadening of a sharp δ18O transition due to molecular diffusion is discussed. Since this broadening is larger than the observed width of the transition, we discuss the possibility of a mechanism that can produce stratigraphic disturbances on a small scale. This mechanism is based on a calculation of the compression of horizontal layers which have equal density but different viscosities.
format Conference Object
author Staffelbach, T.
Stauffer, B.
Oeschger, H.
author_facet Staffelbach, T.
Stauffer, B.
Oeschger, H.
author_sort Staffelbach, T.
title A detailed analysis of the rapid changes in ice-core parameters during the last ice age
title_short A detailed analysis of the rapid changes in ice-core parameters during the last ice age
title_full A detailed analysis of the rapid changes in ice-core parameters during the last ice age
title_fullStr A detailed analysis of the rapid changes in ice-core parameters during the last ice age
title_full_unstemmed A detailed analysis of the rapid changes in ice-core parameters during the last ice age
title_sort detailed analysis of the rapid changes in ice-core parameters during the last ice age
publisher International Glaciological Society
publishDate 1988
url https://boris.unibe.ch/158762/1/a-detailed-analysis-of-the-rapid-changes-in-ice-core-parameters-during-the-last-ice-age.pdf
https://boris.unibe.ch/158762/
geographic Greenland
geographic_facet Greenland
genre Annals of Glaciology
Dye 3
Dye-3
Greenland
Greenland ice cores
ice core
genre_facet Annals of Glaciology
Dye 3
Dye-3
Greenland
Greenland ice cores
ice core
op_source Staffelbach, T.; Stauffer, B.; Oeschger, H. (1988). A detailed analysis of the rapid changes in ice-core parameters during the last ice age. Annals of glaciology, 10, pp. 167-170. International Glaciological Society 10.3189/S0260305500004377 <http://dx.doi.org/10.3189/S0260305500004377>
op_relation https://boris.unibe.ch/158762/
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.3189/S0260305500004377
container_title Annals of Glaciology
container_volume 10
container_start_page 167
op_container_end_page 170
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